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Full Equations (FEQ) Model for the Solution of the Full, Dynamic Equations of Motion for One-Dimensional Unsteady Flow in Open Channels and Through Control Structures

U.S. GEOLOGICAL SURVEY WATER-RESOURCES INVESTIGATIONS REPORT 96-4240

Figure 6

Figure 6. Example of a strongly meandering stream for illustration of the
approximations of curvilinearity used in the Full EQuations model.

U.S. GEOLOGICAL SURVEY WATER-RESOURCES INVESTIGATIONS REPORT 96-4240

Figure 6

Figure 6. Example of a strongly meandering stream for illustration of the approximations of curvilinearity used in the Full EQuations model.

Figure 6. Example of a strongly meandering stream for illustration of the
approximations of curvilinearity used in the Full EQuations model.